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 Mendip
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 Mendip
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 Biodiversity of eastern
 Mendip
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 Biodiversity of western
 Mendip
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Quarrying and geodiversity
"the Mendips are a classical geological site and the beauty that we see today, and wealth of the wildlife – not to mention the famous caves and pot-holes – depend on the particular geological processes that have shaped the land".
William Waldegrave – Minister of State responsible for nature conservation 1985
In "New Sites for Old – a students guide to the Geology of the East Mendips".

The Mendips have a rich 'geodiversity' which means there is a large range of rock types exposed in a small area. This superb diversity of rock types, ranging from Silurian to Jurassic in age, are exposed in many natural rock outcrops, particularly in the western Mendips where the limestone gorges and caves at Cheddar and Wookey are national tourist icons. On eastern Mendip, natural rocky outcrops are largely confined to the intimate twisting largely wooded valleys and quarries.

Outcrop of the Black Rock Limestone, Dolbury, Churchill

These natural exposures have been augmented by numerous quarries which significantly increase the local geodiversity. Many key geological sites, especially in eastern Mendip are in quarries. The most important sites have been designated as Sites of Special Scientific Interest (SSSI's) on the basis of their biological, geological or geomorphological significance. Several quarries, including the disused quarries at Vallis Vale and Great Elm, and the operational or dormant quarries at Cloford, Holwell, Moon's Hill and Cook's Wood Quarry, have this designation. Further details can be found in the Natural England website at www.naturalengland.org.uk/

Some sites, notably at Tedbury Camp Quarry, have been cleaned up in the past to allow safe access and display the geological features to their best advantage.

The Jurassic unconformity at Tedbury Camp Quarry, a geological SSSI



  Quarries offer several advantages for studying geology:
  • They increase the 'geodiversity' of a region
  • They have fresh broken faces which clearly display the rocks
  • The absence of vegetation allows the rocks to be clearly seen
  • Quarrying opens up new exposures where rocks would not otherwise be seen
  • They often expose a range of rock types


Because of their superb exposures, Mendip quarries have attracted the interest of geologists since geology began as a science in the early 19th century. The classic unconformity section exposed in quarries at Vallis Vale was described by Sir Henry de la Beche in the world's first geological survey memoir in 1846. Another early scientist was Charles Moore who in the 1850s and 60s, examined the quarries at Holwell where he found deep fissures in the Carboniferous Limestone infilled with younger Triassic and Jurassic material. This material contained numerous remains of reptiles and early mammals. He also discovered the Silurian igneous rocks at the core of the Beacon Pericline, which led to the development of Moon's Hill, Downhead and other hard rock quarries.

Vallis Vale in 1900. The Jurassic unconformity is clearly seen in the background, along with the narrow gauge railway line used to haul stone to Hapsford.

In recognition of their geological value, in recent times the Mendip quarry companies have developed a very close and proactive relationship with visiting groups and the public, probably better co-ordinated than any other area in the UK. In particular, Hanson pioneered a visitor friendly approach with their East Mendip Study Centre. Foster Yeoman Ltd. (now taken over by Aggregate Industries), the operator of Torr Works quarry has also been innovatory and, like Hansons has offered pre-booked visits to individual members of the public. Although these services are geared mainly to schools and colleges, geological and other interest groups are also hosted. Several quarry companies are combining forces to invest in a new education centre, which is being planned just south of Stoke St Michael.

The quarry companies have also facilitated a 'Geodiversity Audit of Active Aggregates Quarries' in the region, including Whatley, Colemans, Torr Works, Gurney Slade, Halecombe, Moon's Hill and Dulcote quarries. In 2004, detailed examination of numerous geological features at each of these sites was recorded and reported and is available as a CD from Somerset County Council (see their website for details).

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